2021
DOI: 10.1029/2021gl097010
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Stratospheric Gravity Waves as a Proxy for Hurricane Intensification: A Case Study of Weather Research and Forecast Simulation for Hurricane Joaquin

Abstract: Tropical cyclones (TCs) are among the most destructive natural weather phenomena and can cause extensive damage to coastal countries and regions. Close monitoring and accurate forecasts of the tracks and intensity of TCs are needed to reduce human and financial losses.Tropical cyclones are powered by latent heating, mainly from strong updrafts in the eyewall (Charney & Eliassen, 1964;Emanuel, 1986;Kuo, 1965), and latent heat release in the storm is responsible for the dynamical structure and intensity change o… Show more

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Cited by 5 publications
(10 citation statements)
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References 49 publications
(88 reference statements)
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“…The absolute errors of the LR and LSTM models are 0.067 (0.087) and 0.135 (0.045), respectively, when the ASGWs-A is smaller (larger) than 0.5, which shows that the relationship between the ASGWs-A and CI-85 is primarily linearly (nonlinear) when the SGWs are weak (strong); therefore, the role of nonlinear interaction cannot be ignored, especially for strong SGWs. The results from the models are thus sufficiently accurate for the SGWs to be used as a proxy for the CI, consistent with Wu et al (2021).…”
Section: Relationship Between Sgws and Convectionsupporting
confidence: 67%
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“…The absolute errors of the LR and LSTM models are 0.067 (0.087) and 0.135 (0.045), respectively, when the ASGWs-A is smaller (larger) than 0.5, which shows that the relationship between the ASGWs-A and CI-85 is primarily linearly (nonlinear) when the SGWs are weak (strong); therefore, the role of nonlinear interaction cannot be ignored, especially for strong SGWs. The results from the models are thus sufficiently accurate for the SGWs to be used as a proxy for the CI, consistent with Wu et al (2021).…”
Section: Relationship Between Sgws and Convectionsupporting
confidence: 67%
“…Wu et al. (2021) argued that the gravity waves (like those in area B) may be used as a proxy for typhoon intensity, and we raise the question as to whether the SGWs‐A with similar wave parameters to the SGWs‐B influence the intensity of convection (CI) in area A.…”
Section: Influence Of the Sgws On Convectionmentioning
confidence: 81%
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